hydrophysicsФундаментальная и прикладная гидрофизикаFundamental and Applied Hydrophysics2073-66732782-5221St. Petersburg Research Center of the Russian Academy of Sciences10.59887/2073-6673.2024.17(1)-4hydrophysics-1300Research ArticleГИДРОФИЗИЧЕСКИЕ И БИОГЕОХИМИЧЕСКИЕ ПОЛЯ И ПРОЦЕССЫHYDROPHYSICAL AND BIOGEOCHEMICAL FIELDS AND PROCESSESАнализ мезомасштабных фронтальных зон Норвежского моря по спутниковым наблюдениям и данным реанализа в мае 2011–2020 гг.Analysis of mesoscale frontal zones of the Norwegian Sea based on satellite observations and reanalysis data in May 2011–2020https://orcid.org/0000-0002-2089-158XКоникА. А.KonikA. A.

Александр Александрович Коник, младший научный сотрудник, кандидат географических наук

117997; Нахимовский проспект, д. 36; Москва

Scopus AuthorID: 57203864647

117997; 36 Nakhimovsky Prosp.; Moscow

Scopus AuthorID: 57203864647

konikrshu@gmail.comhttps://orcid.org/0000-0001-6820-0533АтаджановаО. А.AtadzhanovaO. A.

Оксана Алишеровна Атаджанова, научный сотрудник, кандидат географических наук

117997; Нахимовский проспект, д. 36; Москва;  299011; ул. Капитанская, д. 2; Севастополь

117997; 36 Nakhimovsky Prosp.; Moscow; 299011; 2 Kapitanskaya Str.; Sevastopol

oksana.atadzhanova@gmail.comhttps://orcid.org/0000-0002-8863-4133СентябовЕ. В.SentyabovE. V.

Евгений Валериевич Сентябов, старший научный сотрудник, кандидат географических наук

183038; ул. Академика Книповича, д. 6; Мурманск

Scopus AuthorID: 14520596600; WoS AuthorID: AES-2062–2022

183038; 6 Akademika Knipovicha Str.; Murmansk

Scopus AuthorID: 14520596600; WoS AuthorID: AES-2062–2022

esenty@yandex.ruИнститут океанологии им. П.П. Ширшова РАНРоссияShirshov Institute of Oceanology, Russian Academy of SciencesRussian FederationИнститут океанологии им. П.П. Ширшова РАН; Морской гидрофизический институт РАНРоссияShirshov Institute of Oceanology, Russian Academy of Sciences; Marine Hydrophysical Institute, Russian Academy of SciencesRussian FederationПолярный филиал Всероссийского научно-исследовательского института рыбного хозяйства и океанографииРоссияPolar Branch of the Russian Federal Research Institute Fisheries and OceanographyRussian Federation2024210420241715262Copyright © Коник А.А., Атаджанова О.А., Сентябов Е.В., 20242024Коник А.А., Атаджанова О.А., Сентябов Е.В.Konik A.A., Atadzhanova O.A., Sentyabov E.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://hydrophysics.spbrc.ru/jour/article/view/1300

   Цель исследования — сравнение рассчитанных на основе спутниковых наблюдений и данных реанализа горизонтальных градиентов температуры в области поверхностных проявлений мезомасштабных фронтальных зон и для всей акватории Норвежского моря в период начала нагульных миграций пелагических рыб в мае 2011–2020 гг.

   На основе среднемесячных данных температуры MODIS/Aqua, GHRSST OSTIA и CMEMS GLORYS12v1 рассчитаны поля среднемесячных и десятилетних горизонтальных градиентов на поверхности Норвежского моря. Выполнено сравнение полученных десятилетних оценок градиентов температуры с их средними климатическими значениями. Выявлено, что в большинстве данных регистрируются поверхностные проявления основных фронтальных зон Норвежского моря. На основе уникальных in situ наблюдений проведена валидация полей температуры в области Исландско-Фарерской фронтальной зоны. Показано, что для анализа фронтальных зон Норвежского моря наиболее предпочтительно использование полей температуры GHRSST OSTIA. Полученные физико-географические особенности мезомасштабных фронтальных зон возможно использовать для оценки связи с миграциями пелагических рыб в Норвежском море.

   The aim of this study is to compare the horizontal temperature gradients calculated based on satellite observations and reanalysis data in the area of mesoscale frontal zones’ surface manifestations, both for the entire Norwegian Sea and during the onset of pelagic fish spawning migrations in May from 2011 to 2020.

   Using monthly average temperature data from MODIS/Aqua, GHRSST OSTIA, and CMEMS GLORYS12v1, the fields of monthly and decade-long horizontal gradients on the surface of the Norwegian Sea were derived. A comparison was made between the decade-long temperature gradient estimates and their mean climatic values. The majority of the data show surface manifestations of the main frontal zones in the Norwegian Sea. Validation of temperature fields in the area of the Iceland-Faroe Frontal Zone was conducted based on unique in situ observations. It was demonstrated that for the analysis of the frontal zones in the Norwegian Sea, using the temperature fields of GHRSST OSTIA is most preferable. The obtained physico-geographical characteristics of mesoscale frontal zones could be used to assess their relationship with pelagic fish migrations in the Norwegian Sea.

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The authors declare that there are no conflicts of interest present.